Revisiting turbulence small-scale behavior using velocity gradient triple decomposition

TL;DR

This study revisits turbulence small-scale behavior using a triple decomposition of the velocity-gradient tensor, revealing the dominant role of shear and providing deeper insights into intermittency and flow structures.

Contribution

It introduces a triple decomposition approach to analyze velocity-gradient tensors, offering a more detailed understanding of turbulence small-scale features beyond traditional methods.

Findings

Shear dominates contributions to velocity-gradient magnitude at all Reynolds numbers.

Intermittency in enstrophy is mainly due to shear, not rigid-body rotation.

Triple decomposition enhances understanding of turbulence small-scale dynamics.

Abstract

Turbulence small-scale behavior has been commonly investigated in literature by decomposing the velocity-gradient tensor ($A_{ij}$) into the symmetric strain-rate ($S_{ij}$) and anti-symmetric rotation-rate ($W_{ij}$) tensors. To develop further insight, we revisit some of the key studies using a triple decomposition of the velocity-gradient tensor. The additive triple decomposition formally segregates the contributions of normal-strain-rate ($N_{ij}$), pure-shear ($H_{ij}$) and rigid-body-rotation-rate ($R_{ij}$). The decomposition not only highlights the key role of shear, but it also provides a more accurate account of the influence of normal-strain and pure rotation on important small-scale features. First, the local streamline topology and geometry are described in terms of the three constituent tensors in velocity-gradient invariants' space. Using DNS data sets of forced isotropic turbulence, the velocity-gradient and pressure field fluctuations are examined at different Reynolds numbers. At all Reynolds numbers, shear contributes the most and rigid-body-rotation the least toward the velocity-gradient magnitude ($A^2$). Especially, shear contribution is dominant in regions of intermittency (high values of $A^2$). It is also shown that the high-degree of enstrophy intermittency reported in literature is due to the shear contribution toward vorticity rather than that of rigid-body-rotation. The study also provides an explanation for the absence of intermittency of the pressure-Laplacian, despite the strong intermittency of enstrophy and dissipation fields. Overall, it is demonstrated that triple decomposition offers unique and deeper understanding of velocity-gradient behavior in turbulence.